2.1 Geology and Engineering Flashcards

1
Q

Engineering methodology

A

Step 1: Problem definition
Step 2: Analysis & Design
Step 3: Construction
Step 4: Operation
Step 5: Decommissioning

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2
Q

Overall Goal of Methodology

A

Site Characterization: provide a model of the sub surface to allow evaluation of designs to meet specific engineering objectives.

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3
Q

Essential Geology to consider?

A
  • Stratigraphy
  • Sedimentology
  • Geo-morphology
  • Structure
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4
Q

Stratigraphy

A
  • Sequence of Layers
  • Order of deposition
  • Lateral variation
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5
Q

Sedimentology

A

De-positional processes (wind, water, ice, etc.)

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6
Q

Geo-morphology

A
  • Land forms
  • De-positional
  • Erosional
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7
Q

Structure

A

Deformation after deposition (folding, faulting, jointing)

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8
Q

Composition (Mineralogy)

A

Scientific study of the chemistry, crystal structure, and physical properties of minerals.
Silicate minerals (quartz, feldspars, clays) vs non-silicates (carbonates, oxides, sulphides).

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9
Q

Composition (Petrology)

A

Study of rocks (igneous, metamorphic, and sedimentary) - and the processes that form and transform them

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10
Q

Burial History

A
  • Have the particles been reoriented and packed closer together? (compaction increases strength and reduced porosity)
  • Have the fluids been expelled? (Consolidation increases strength and reduces porosity)
  • Is there any mineral precipitation? (Cementation increases strength and reduces porosity)
  • Are the grains joined by cement? (lithification increases strength and reduces porosity)
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11
Q

Groundwater (Regional and Local Systems)

A

Flow occurs on many scales (m to hundreds of km)

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12
Q

Groundwater (Aquifers and Aquitards)

A
  • units based on permeability (how easily a fluid can move through the unit), not stratigraphy.
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13
Q

Fundamental properties

A
  • Permeability: the ability to transmit fluid through the pore spaces
  • Compressibility: the volume change response to load (stress)
  • Strength: the ability to carry a load (stress)
  • Density: mass/unit volume
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14
Q

Structure of the earth: inside out

A
  1. Inner core
  2. Core
  3. Mantle
  4. Crust
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15
Q

Inner core

A
  • Mostly solid iron and nickel
  • Very high pressures
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16
Q

Outer core

A
  • Liquid iron and nickel
  • heated by the radioactive decay of U and Th
17
Q

The mantle

A
  • thickest layer
  • mostly iron, magnesium, and silicon
18
Q

The crust

A
  • extremely thin, cold and brittle
  • composed of siica, aluminum, and oxygen
19
Q

What are minerals?

A

Naturally occurring in organic crystalline solid that has definite physical and chemical properties.

20
Q

What are rocks?

A

Naturally formed consolidated material composed of a mixture of minerals.

21
Q

What is the most abundant and important rock forming mineral?

22
Q

What minerals are important to engineers because they are strongly resistant to weathering and occur in most soils?

A

Quartz and feldspars

23
Q

Igneous rocks

A

Material origin: Crystallized from molten magma
Environment: Underground; and as lava flows
Texture: Mosaic of interlocking crystals
Structure: Massive (structure-less)
strength: Uniform high strength
Major types: Granite, Basalt

24
Q

How to identify whether an igneous rock is intrusive or extrusive?

A

The rate at which magma cools which is reflected in the rocks texture

25
Intrusive
Form plutons (also called plutonic rock) that cool and solidify underground slowly - large crystals like granite
26
Extrusive
Magma cools rapidly above surface - small crystals like basalt
27
Metamorphic rocks
Origin: Altered by heat/pressure Environment: Mostly deep inside mountain chains Texture: Mosaic of interlocking crystals Structure: Crystal orientation due to pressure Strength: Variable high; planar weaknesses Major types: schist, gneiss, slate, marble
28
How to identify metamorphic rocks
Unlike the other two types of rocks, metamorphic rocks start as rocks and then are transformed into different rocks.
29
Sedimentary rocks
Origin: Erosional debris on earth's surface Environment: Deposition Basins; mainly sea texture: mostly granular and cemented structure: layered, bedded, and bedding planes strength: variable low; planar weaknesses Major types; sandstone, limestone, clay
30
Cycle of geology
Processes: Land - erosion of rock destruction Marine (ocean, sea) - deposition and forming new sediments Underground - new rocks created and deformed
31
Relationship between geology and engineering
Geological processes continually modify the earths surface, and add to the complexity of ground conditions. All civil engineering works are carried out on or in ground so its properties and processes are very important to understand. - Most rocks encountered by engineers are 10 - 500 M years old and they have been displaced and deformed over time. - Most surface land forms visible today were formed in the last few M years - This time difference is important because the origin of the rocks at surface may bear NO relationship to the present environment
32
Site investigation
Where most engineers will encounter geology - Data collection interpretation of ground conditions - 3D thinking/modeling rendering - Recognition of hazards/difficult ground conditions - Understanding how the geology will impact your design (and budget) - How to manipulate the ground to behave as you need